Results 121 to 130 of about 2,579 (215)
Mesoscale Eddies Reorganize Subsurface Oxygen Minimum Layer in the Subtropical North Atlantic
Abstract Mesoscale eddies play a key role in regulating oceanic physical and biogeochemical environments. However, their influence on vertical oxygen distribution remains poorly constrained by observations. Using 32 years (1993–2024) of in situ oxygen observations from the Bermuda Atlantic Time‐series Study site combined with satellite‐tracked eddies ...
Peiya Zhang +6 more
wiley +1 more source
Observed Multi‐Decadal Acceleration of Globally Averaged Abyssal Ocean Warming
Abstract Given sparse historical data in the deep and abyssal ocean, previously only multi‐decadal temperature trends have been estimated from observations there on a global scale. Full‐depth CTD sampling started circa 1970, with the first decadal global ship‐based survey occupied in the 1990s, and the first regional pilot array of Deep Argo floats ...
Gregory C. Johnson
wiley +1 more source
Abstract Coastal marine heatwaves (MHWs) derived from satellite and blended sea surface temperature (SST) products often disagree, but the magnitude and drivers of this uncertainty remain poorly quantified. Using four daily SST products from 1982 to 2023, we quantify agreement at 9,946 global coastal points using two inter‐product intersection‐over ...
Wenjin Sun +4 more
wiley +1 more source
Marine Heatwave Imprints on Salinity in the Northwest Atlantic
Abstract Marine heatwaves (MHWs) are increasing in frequency and intensity in global boundary current systems such as the Gulf Stream (GS), where ocean circulation regulates upper‐ocean heat and water‐mass properties. We examine temperature–salinity co‐evolution during MHWs in the Northwest (NW) Atlantic using satellite observations and ocean ...
Natalie Stamper +2 more
wiley +1 more source
Reduced Wind Power on Oceanic Near‐Inertial Internal Waves in a Warming Climate
Abstract Wind power on oceanic near‐inertial internal waves (WI ${W}_{\mathrm{I}}$) is one of the major energy sources to sustain ocean turbulent diapycnal mixing. However, its response to global warming remains poorly understood. Using a high‐resolution climate simulation that simulates WI ${W}_{\mathrm{I}}$ reasonably well, we show that under a high ...
Shuyi Huang +5 more
wiley +1 more source
Evaporation and Cold Pools Beneath Trade Cumulus Clouds
Abstract The sources of air and water vapor in the tropical trade‐wind Atlantic subcloud boundary layer (SBL) are analyzed using in situ measurements of temperature, specific humidity, and stable water isotopologues (HDO and H218O) from shipboard observations in January‐February 2020.
Estefanía Quiñones Meléndez +6 more
wiley +1 more source
Opposite Trends of Eddy Kinetic Energy in the Tropical Indo‐Pacific Ocean Since the 1990s
Abstract Oceanic mesoscale eddies are pivotal in redistributing mass and heat. Despite a warming‐induced increase in global oceanic stratification, previous studies have reported a global increase in mesoscale eddy activity, particularly in eddy‐rich regions, pointing to a complex and regionally contingent response to climate change.
Xinying Guo +6 more
wiley +1 more source
Weak 21st‐Century AMOC Response to Greenland Meltwater in a Strongly Eddying Ocean Model
Abstract Climate models project that the Atlantic Meridional Overturning Circulation (AMOC) will weaken in the 21st century, but the magnitude is highly uncertain. Some of this uncertainty is structural, as most climate models neglect increasing meltwater from the Greenland ice sheet and do not explicitly capture mesoscale ocean eddies.
Oliver Mehling, Henk A. Dijkstra
wiley +1 more source
Observing mesoscale eddy effects on mode-water subduction and transport in the North Pacific. [PDF]
Xu L, Li P, Xie SP, Liu Q, Liu C, Gao W.
europepmc +1 more source
Calibration of a Neural Network Ocean Closure for Improved Mean State and Variability
Abstract Global ocean models exhibit biases in the mean state and variability, particularly at coarse resolution, where mesoscale eddies are unresolved. To address these biases, parameterization coefficients are typically tuned ad hoc. Here, we formulate parameter tuning as a calibration problem using Ensemble Kalman Inversion (EKI).
Pavel Perezhogin +2 more
wiley +1 more source

